逆冲断层 meaning in English
reverse thrust
reversed fault
reversedfault
thrust fault
thrustfault
Examples
- The reverse structure appears in three styles . they are regional structure reverse occurred as angle unconformity between paleogene and neogene , thrush fault and local reverse structures
反转构造以三种形式出现，即上下第三系之间角度不整合的区域性构造反转，逆冲断层，局部构造的反转。 - The pre - jurassic basement of hefei basin was composed of thrusts . indosinian foreland thrusts in pre - jurassic bedrocks of the basin increase towards the tan - lu fault zone , indicating indosinian activity of the fault zone
合肥盆地在印支期的前侏罗纪基底主要表现为大别造山带前陆逆冲推覆构造，由一系列逆冲断层和逆冲岩片所组成。 - Kongxi buried hill shows following features in the seismic profiles : the structures are asymmetric . there is flexural syncline on the east side and a monocline on the west side . asymmetric repetition of stratigraphic units is present in the drill wells and the dips of beds and faults are gentle . the permo - carboniferous system of both sides almost lie in the same slope and the events of cambrian or upper proterozoic are continuous from east to west . the phenomenas suggest that kongxi buried hill could be a thrust belt been traced which consists of reverse faults . the imbricate faults mainly effect pre - jurassic strata . there are obvious angular unconformity between jurassic - cretaceous system and paleozoic involved deformation of thrust . the thrust front in some place has cut off the beds of jurassic - cretaceous system . the structural style of the thrust structure changes along the strike of the kongxi buried hill
地震和钻井资料揭露的孔西构造带前第三系潜山的地质特征可以归纳为：构造带总体上不对称构造带内部有地层重复现象石炭二叠系地层的位置明显高于两侧的同一地层的高度。用由34条向东倾斜的逆冲断层组成的叠瓦扇构造模式能够比较合理地解释上述地质特征。该带向东倾斜的逆冲叠瓦状断层组主要影响前侏罗系地层，侏罗白垩系与卷入逆冲构造变形的古生界地层之间有明显的角度不整合。 - In order to explain the spatial and temporal distribution of volcanic rocks with different ages and tectonic regimes , one archipelagic model is proposed . the shizong - mile zone in se yunnan was composed of different tectonic blocks with different ages , lithological features and provenances , and contacted each other by a shear zone
滇东南师宗弥勒带主要以一系列逆冲断层为骨架，剪切包容古生界、少量三叠系和元古界地层的构造岩块、以及火山岩构造岩片，共同构成一个由多条断层控制不同时代、不同性质构造岩块的混杂带。